Structure and Composition

Highlights

  • Old growth differs significantly from younger growth in structural and compositional attributes that include a multi-aged and multi-layered canopy, horizontal patchiness with canopy gaps, numerous large snags and logs, two or more tree species, wide uneven tree spacing, hummocky microtopography of the forest floor, and increased understory production. In comparison, forests initiated by forest harvesting and planting of a single tree species are often relatively simple and homogeneous in structure and composition

Overview

Old growth forests are complex natural systems, in which all parts are connected, and death is as important as life in sustaining the system. At the time a tree dies, it has only partially fulfilled its potential ecological function. Live trees provide source material for the other key structural components of old growth forests including snags, logs on the ground, logs in streams and the forest floor.

Old growth differs significantly from younger growth by structural and compositional attributes that include large old living trees, a wide range of tree sizes and ages, a multi-layered canopy, horizontal patchiness with canopy gaps resulting from the mortality of single or small groups of trees, numerous large snags and large diameter long downed logs, two or more tree species, wide uneven tree spacing, hummocky microtopography of the forest floor, and increased understory production (Pojar et al., 1992; Price et al., 2020). Driven by gap dynamics, the forest canopy continuously renews itself and complex canopy structure is maintained (Daniels and Gray, 2006). Old growth attributes develop faster on moist, productive sites than drier, poor sites, for example good sites develop a wider range of tree sizes earlier than poor sites (Franklin et al., 1981).

Live and dead trees

Trees in old growth forests are individualistic, with their characteristics shaped over the centuries by their genetics, competition with nearby trees, the effects of disturbances such as storms, diseases, and insects, and site conditions (Franklin et al., 1981). In contrast, many mid-seral and mature forests are dense, dark, and uniform with little understory. Those initiated by forest harvesting and planting of a single tree species can be particularly homogeneous and simple in structure and composition.

There are typically more standing dead trees (snags) and large fallen trees in old growth than in younger forests, although this depends on location and species. Snags of western redcedar can remain standing for 75 to 125 years and Douglas-fir snags typically persist for 50 to 75 years (Franklin et al., 1981). One special attribute of old growth forests (and natural second growth) is that they contain snags in varying stages of decay, whereas young managed stands do not.

Complex Stand Structure. Photo by Sherry Kirkvold

Logs

Logs on the forest floor in old growth stands can contain huge amounts of biomass (up to 418 tonnes ha-1) with greater amounts on lower slope streamside sites than dry sites (Franklin et al., 1981). They decompose slowly, losing only about 40% of their original density after 150-200 years. Decomposition models estimate that it takes 480 to 580 years for an 80 cm diameter Douglas-fir to become 90% decayed (Franklin et al., 1981).
Large log in an old-growth stand. Photo by Sherry Kirkvold

Understory trees and plants

Tree regeneration and growth of understory plants including cryptogams (mosses, lichens, liverworts) is facilitated within the canopy gaps of old growth forests. There is generally greater patchiness of understory tree seedlings, shrubs, and herbs in old growth forests than younger, less structurally diverse stands. This is related to an uneven pattern of openings and shaded areas as well as provision of new substrate.

Read more about cryptogams.